NUMERICAL EXPERIMENTS ON COUPLED MAGMATISM-MANTLE CONVECTION SYSTEM - IMPLICATIONS FOR MANTLE EVOLUTION AND ARCHEAN CONTINENTAL CRUSTS

被引：15

作者：

OGAWA, M ^{[1
]}

机构：

[1] UNIV TOKYO,FAC SCI,INST GEOPHYS,TOKYO 113,JAPAN

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS | 1988年 / 93卷 / B12期

关键词：

D O I：

10.1029/JB093iB12p15119

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

引用

页码：15119 / 15134

页数：16

共 50 条

[1] A NUMERICAL-MODEL OF A COUPLED MAGMATISM MANTLE CONVECTION SYSTEM IN VENUS AND THE EARTHS MANTLE BENEATH ARCHEAN CONTINENTAL CRUSTS
OGAWA, M
ICARUS, 1993, 102 (01) : 40 - 61
[2] A bifurcation in the coupled magmatism-mantle convection system and its implications for the evolution of the Earth's upper mantle
Ogawa, M
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1997, 102 (3-4) : 259 - 276
[3] Coupled magmatism-mantle convection system with variable viscosity
Ogawa, M
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[4] Two-stage evolution of the Earth's mantle inferred from numerical simulation of coupled magmatism-mantle convection system with tectonic plates
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[5] Evolution of the interior of Mercury influenced by coupled magmatism-mantle convection system and heat flux from the core
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[6] The Four-Stage Evolution of Martian Mantle Inferred From Numerical Simulation of the Magmatism-Mantle Upwelling Feedback
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[7] Coupled evolution of Archean continental crust and subcontinental lithospheric mantle
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[8] Thermochemical regime of the early mantle inferred from numerical models of the coupled magmatism-mantle convection system with the solid-solid phase transitions at depths around 660 km
Ogawa, M
Nakamura, H
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[9] Plume and arc magmatism in the Abitibi subprovince: Implications for the origin of Archean continental lithospheric mantle
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PRECAMBRIAN RESEARCH, 2009, 168 (1-2) : 4 - 22
[10] EFFECTS OF CHEMICAL FRACTIONATION OF HEAT-PRODUCING ELEMENTS ON MANTLE EVOLUTION INFERRED FROM A NUMERICAL-MODEL OF COUPLED MAGMATISM MANTLE CONVECTION SYSTEM
OGAWA, M
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